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  • 2000-2004  (11)
  • 1965-1969  (1,075)
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  • 1945-1949  (21)
  • 1967  (1,075)
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  • 1
    Monograph available for loan
    Monograph available for loan
    [Moskva] : Izdatel'stvo Moskovskogo Universiteta
    Call number: AWI G3-24-95658
    Type of Medium: Monograph available for loan
    Pages: 302 Seiten , Illustrationen
    Language: Russian
    Note: СОДЕРЖАНИЕ Предисловие Введение Глава 1. Процессы замерзания - таяния горных пород и свойства мерзлых пород Мерзлые горные породы - многофазные и многокомпонентные системы Содержание жидкой воды и льда в мерзлых породах. Температурные условия замерзания воды в породах Свойства мерзлых горных пород Типы замерзания воды в горных породах Физические процессы в оттаивающих горных породах Изменение объема мерзлых пород и образование трещин Основные закономерности строения мерзлых горных пород Глава II. Сезонная и вечная мерзлота Сезонная мерзлота Вечная мерзлота Глава III. Криогенез как процесс литогенеза Зоны охлаждения Земли как зоны особого типа литогенеза Лед как минерал . Типы подземного льда Место криолитоrенеза в общей системе литогенеза Глава IV. Криогенные горные породы Криолиты - ледяные мономинеральные породы Криолититы - льдистые полиминеральные породы Криоэлювииты - вторичные продукты криолитогенеза Глава V. Типы криолитогенеза Эпиrенетический тип криолитогенеза Сингенетический тип криолитогенеза О термокарсте Глава VI. География криолитогенеза Зональность процессов криолитогенеза Криолитогенез как региональное явление Мерзлотно-геологическое районирование области вечной мерзлоты в СССР Заключение Литература , English translation of Table of Contents Preface Introduction Chapter 1. Freezing processes - thawing of rocks and properties of frozen rocks Frozen rocks - multiphase and multicomponent systems Content of liquid water and ice in frozen rocks. Temperature conditions for freezing water in rocks Properties of frozen rocks Types of water freezing in rocks Physical processes in thawing rocks Changes in the volume of frozen rocks and the formation of cracks Basic patterns of the structure of frozen rocks Chapter II. Seasonal and permafrost Seasonal permafrost Permafrost Chapter III. Cryogenesis as a process of lithogenesis Cooling zones of the Earth as zones of a special type of lithogenesis Ice as a mineral Types of underground ice Place of cryolithogenesis in the general system of lithogenesis Chapter IV. Cryogenic rocks Cryolites - icy monomineral rocks Cryolites - icy polymineral rocks Cryoeluviites - secondary products of cryolithogenesis Chapter V. Types of cryolithogenesis Epi-genetic type of cryolithogenesis Syngenetic type of cryolithogenesis About thermokarst Chapter VI. Geography of cryolithogenesis Zoning of cryolithogenesis processes Cryolithogenesis as a regional phenomenon Permafrost-geological zoning of the permafrost region in the USSR Conclusion Literature , In kyrillischer Schrift
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  • 2
    Monograph available for loan
    Monograph available for loan
    Düsseldorf : Econ-Verlag
    Call number: AWI E2-23-95526
    Description / Table of Contents: Pavel Gordijenko hat sein Leben der Polarforschung gewidmet. Er machte auf Eisbrechern Expeditionen mit, überwinterte auf Polarstationen, führte Eisdriftfahrten, Eiserkundungsflüge und Kreuzfahrten vor den arktischen Küsten durch. Er gibt in diesem Buch weitreichende Einblicke, warum, wie und mit welchen Ergebnissen die sowjetischen Forscher die Geheimnisse des Nordpols und des riesigen Meeres, das diesen bemerkenswerten Punkt umgibt, ergründen konnten. In dem Vorwort zu diesem zuerst in deutscher Sprache erschienenen Werk vermerkt der sowjetische Wissenschaftler: »Ich habe mich entschlossen, in diesem Buch die Hauptergebnisse der wissenschaftlichen Forschungsarbeiten sowjetischer Polarforscher in der Zentralarktis allgemein verständlich darzustellen. Um dieser schwierigen Aufgabe gerecht zu werden, habe ich mich entschieden, nur die Forschungsarbeiten der letzten 25 Jahre zu behandeln. Ich würde jedoch meine Aufgabe als nur teilweise gelöst empfinden, wenn ich mich auf eine trockene Darlegung der wissenschaftlichen Forschungsergebnisse beschränken und nichts davon berichten würde, wie Menschen der verschiedensten Berufe in der Arktis leben und arbeiten, unter welchen Bedingungen und unter welchen Mühen sie hier ihre Kenntnisse sammeln, mit welchen Gefahren und Entbehrungen ihre Arbeit manchmal verbunden ist. Ich werde deshalb in meinem Buch auch einige Episoden erzählen, die teils ungewöhnliche und bedeutungsvolle Ereignisse und Vorkommnisse beinhalten, teils jedoch auch Dinge, die für einen Polarforscher nichts Ungewöhnliches sind. Ich schreibe hier einerseits als Augenzeuge, andererseits als Beteiligter.« So ist ein Buch entstanden, das eine Reihe der faszinierenden Phänomene der Arktis verständlich macht, etwa die Entstehung des Nordlichts, die Bewegung des Eises und die gewaltigen, Auswirkungen der Meeresströmungen, ein Buch, das zudem Einblicke gibt, wie die verschiedenen .Forschergruppen - Hydrologen, Aerologen, Meteorologen,Geographen,Geologen, Ozeanographen, Physiker u. a. mehr - zusammenarbeiten, um die Arktis als Lebensraum für den Menschen zu erschließen, neue Verkehrswege zu finden, die Wettervorhersage zu vervollkommnen, vielleicht sogar das Klima zu beeinflussen. Polarforschung ist trotz aller technischen Vervollkommnung noch immer eines der großen Abenteuer unseres Jahrhunderts. Es bezieht seine Faszination aus dem Kampf des Menschen mit »ihrer Majestät - der arktischen Natur«, in der es Siege und Niederlagen gibt, von dem wir aber wissen, »daß die rauhe Natur dem Menschen allmählich untertan wird und ihre Kräfte ihm schon zu dienen beginnen«,
    Type of Medium: Monograph available for loan
    Pages: 350 Seiten , Illustrationen , 1 Beilage
    Edition: 1. Auflage
    Language: German
    Note: INHALTSVERZEICHNIS Vorwort 1. Kapitel DER KLEINSTE UND RAUHESTE OZEAN Das Nördliche Eismeer und der Nordpol Was ist die Arktis? Und dieser Ozean ist voller Leben Gutes oder »schlechtes« Wetter Die Rauheit des Wetters und Möglichkeiten der menschlichen Tätigkeit Die Polarländer - Antipoden 2. Kapitel VON DER LEGENDE ZUR WISSENSCHAFTLICHEN ERKENNTNIS In alten Zeiten Die Idee der Nordost-Passage Spitzbergen und Nowaja Semlja Erforschung der asiatischen Küsten des Nördlichen Eismeeres Die Große Nordexpedition Der Begründer der Polarozeanographie Der erste Versuch einer Fahrt zum Pol Die geheimnisvolle Insel Russen in Amerika Transarktisfahrten zum Nordpol Die neue Technik im Dienst der arktischen Wissenschaft Die Entdeckung von Sewernaja Semlja Die Hauptergebnisse der russischen Polarforschung bis zur Oktoberrevolution 3. Kapitel IN DER ARKTIS HEUTE Die ersten Etappen sowjetischer Arktisforscher Die »Sibirjakow« und die Entwicklung des Nördlichen Seeweges Die weitere Forschung Die weißen Flecke von der Landkarte der Zentralarktis verschwinden Polarstationen - ständige Vorposten der arktischen Wissenschaft Die Arktis ist unerbittlich Dem Tod um Haaresbreite entgangen Ein »bedingter Reflex« führt zu einer mißlichen Lage Vorbereitungen für eine Bergbesteigung Aus dem Bergsteiger-Tagebuch Der Gipfel ist bezwungen Von der Küste ins offene Meer Die Expeditionen »Sewer« in hohen nördlichen Breiten Eine »Springgruppe« am Pol 4. Kapitel MEHR ALS ZWANZIG JAHRE DRIFT AM POL Kampf mit den Elementen Alte und neue wissenschaftliche Probleme Zeit, Trajektorien, Kilometer Neue Geräte und Ausrüstungen Die Menschen auf den »Nordpol«-Stationen und ihre Arbeit Unvergeßliche Tage auf der Drift Die Polarnacht Entdeckungen im Meer 5. Kapitel NEUE ZÜGE DER ERDOBERFLÄCHE UNTER WASSER Entdeckungen auf dem Meeresboden Die geologische Geschichte des Meeresbodens 6. Kapitel DIE DRIFT DES EISES IM ARKTISCHEN BECKEN Systematische Beobachtungen Kreisförmige Drift oder direkter Abfluß in den Atlantik? Gewundene Driftlinien der Eisfelder Schleifenkurven in der Eisdrift Drehbewegungen der Eisfelder 7. Kapitel IN DEN TIEFEN DES MEERES UND IN DER FREIEN ATMOSPHÄRE Einige Worte über Wise und Subow. Die Wassermassen und ihre Zirkulation Die Zirkulation der Atmosphäre Durch Atmosphärenforschung zur Wettervorhersage 8. Kapitel ZU KOSMISCHEN HÖHEN Geophysikalische Untersuchungen Magnetische Störungen In den ionisierenden Schichten der Erdatmosphäre »Nordlichter« 9. Kapitel DAS ZIEL IST GREIFBAR, DOCH UNGEWISS Umgestaltung der arktischen Natur Budykos Projekt Andere Pläne zur Änderung des Klimas 10. Kapitel GEBURT EINES NEUEN BERUFES Aufklärungsflüge in der Arktis Das Kartieren der Eisverhältnisse, die Einführung von Isograden und Isolinien Beobachtungen über Unebenheiten der Eisdecke 11. Kapitel VORHERSAGEN - HÖHEPUNKT DER ARKTISFORSCHUNG (Anstelle eines Schlußwortes) Anhang Anmerkungen Tabellen Stichwortverzeichnis
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  • 3
    Monograph available for loan
    Monograph available for loan
    Moskva : Izdatel'stvo "Nauka"
    Call number: AWI G3-23-95528
    Description / Table of Contents: Монография посвящена выявлению взаимосвязи во времени и пространстве Сибирской платформы и Саяно-Байкальской складчатой системы. Основное внимание уделено анализу строения и развития краевых платформенных структур первого порядка, представленных здесь краевым швом, рифейскими миоrеосинклиналями, рифейскими вулканическими поясами, нижнепалеозойскими краевыми прогибами и послепалеозойскими предгорными прогибами. Показано, что рифейские миогеосинклинали Сибири и краевые прогибы ангароленского типа составляют вместе с прогибами уральского и карпатского типов исторический ряд краевых структур платформ, отражающий направленность и стадийность развития, Земли.
    Description / Table of Contents: Translation of the abstract: The monograph is devoted to identifying the relationship in time and space of the Siberian Platform and the Sayan-Baikal fold system. The main attention is paid to the analysis of the structure and development of marginal platform structures of the first order, represented here by the marginal suture, Riphean mioreosynclines, Riphean volcanic belts, Lower Paleozoic foredeeps and post-Paleozoic foredeeps. It is shown that the Riphean miogeosynclines of Siberia and the edge troughs of the Angarolena type, together with the troughs of the Ural and Carpathian types, constitute a historical series of edge structures of platforms, reflecting the direction and stage of development of the Earth.
    Type of Medium: Monograph available for loan
    Pages: 246 Seiten , Illustrationen
    Language: Russian
    Note: ОГЛАВЛЕНИЕ Введение Глава I. История вопроса Глава II. Некоторые особенности дорифейской истории геологического развития юга Восточной Сибири Глава III. Рифейский этап тектонического развития Сибирской платформы Некоторые вопросы стратиграфии отложений позднего докембрия Формации позднего докембрия Основные элементы рифейокой структуры Главные особенности развития краевых структур Сибирской платформы в рифее Глава IV. Нижнепалеозойский этап развития южной части Сибирской платформы и смежных районов Саяно-Байкальской складчатой системы Каледонские формации Формации южной части Сибирской платформы Нижне- и среднекембрийские орогенные формации Саяно-Байкальской области Геосинклинальные формации нижнего палеозоя Саяно-Байкалыской области Послесреднекембрийские орогенные формации Вертикальные ряды формаrщй Саяно-Байкальской области Вертикальные и горизонтальные ряды кембро-силурийюыих формаций Сибирской платформы Горизонтальные ряды нижнекембрийских формаций геосинклинальных и орогенной областей, краевых прогибов и стабильной области Сибирокой платформы Некоторые особенности формиравания кембрийских формаций орогенной области и краевых прогибав Каледонская структура южной части Восточной Сибири Структура южной части Оибцμокой платформы Структура Саяно-Байкалыской области Другие вопросы каледонской тектоники О тектоничеокой природе Ангаро-Ленского и Присаяно-Енисейокого прогибов Цикличность геологического развития юга Восточной Сибири в нижнем палеозое Типы колебательных движений Глава V. Посленижнепалеозойская история развития южной части Сибирской платформы Верхнепалеозойскше и мезозойские структуры Разrвитие южной части Сибирской платформы в кайнозое Современная структура южной части Сибирской платформы Глава VI. Складчатые структуры и разломы краевой системы южной части Сибирской платформы. Механизм и время образования складок Мoрфологические и генетические типы окладчатых структур Механизм образования складчатых структур Время образо,вания складчатых структур Разломы Заключение Литература , Translation of TABLE OF CONTENTS Introduction Chapter I. History of the issue Chapter II. Some features of the pre-Riphean history of the geological development of the south of Eastern Siberia Chapter III. Riphean stage of tectonic development of the Siberian Platform Some questions of stratigraphy of Late Precambrian deposits Late Precambrian formations Basic elements of the Riphean structure The main features of the development of the marginal structures of the Siberian Platform in the Riphean Chapter IV. Lower Paleozoic stage of development of the southern part of the Siberian Platform and adjacent areas of the Sayan-Baikal fold system Caledonian formations Formations of the southern part of the Siberian Platform Lower and Middle Cambrian orogenic formations of the Sayan-Baikal region Geosynclinal formations of the Lower Paleozoic of the Sayan-Baikaly region Post-Middle Cambrian orogenic formations Vertical rows of molds in the Sayan-Baikal region Vertical and horizontal series of Cambro-Silurian formations of the Siberian Platform Horizontal series of Lower Cambrian formations of geosynclinal and orogenic regions, marginal troughs and stable region of the Siberian Platform Some features of the formation of Cambrian formations of the orogenic region and marginal troughs Caledonian structure of the southern part of Eastern Siberia Structure of the southern part of the Oibtso platform Structure of the Sayano-Baikaly region Other issues of Caledonian tectonics On the tectonic nature of the Angara-Lena and Prisayan-Yenisei troughs Cyclicity of geological development of the south of Eastern Siberia in the Lower Paleozoic Types of oscillatory movements Chapter V. Post-Lower Paleozoic history of the development of the southern part of the Siberian Platform Upper Paleozoic and Mesozoic structures Development of the southern part of the Siberian Platform in the Cenozoic Modern structure of the southern part of the Siberian Platform Chapter VI. Folded structures and faults of the marginal system of the southern part Siberian platform. Mechanism and time of fold formation Morphological and genetic types of lamellar structures Mechanism of formation of folded structures Time of formation of folded structures Rifts Conclusion Literature , In kyrillischer Schrift
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  • 4
    Monograph available for loan
    Monograph available for loan
    Moskva : Izdatel'stvo "Nauka"
    Call number: AWI G3-23-95324
    Description / Table of Contents: В сборнике освещаются на основе научного обобщения новых данных геолого-геофизических исследований и глубокого бурения вопросы тектоники, истории развития и нефтегазоносности ряда крупных впадин падин различного типа Западной и Восточной Сибири, а также дается их сравнительная характеристика. Кроме того, в ряде статей приводится детальная характеристика структурно-тектонических особенностей и нефтегазоносности отдельных наиболее характерных впадин указанных районов с целью выявления некоторых общих закономерностей их геологического строения и размещения на их территории месторождений нефти и газа.
    Description / Table of Contents: Translation of the abstract: Based on the scientific generalization of new data from geological and geophysical studies and deep drilling, the collection highlights the issues of tectonics, the history of development and oil and gas potential of a number of large depressions of depressions of various types in Western and Eastern Siberia, and also gives their comparative characteristics. In addition, a number of articles provide a detailed description of the structural-tectonic features and oil and gas potential of some of the most characteristic depressions of these areas in order to identify some general patterns of their geological structure and the location of oil and gas fields on their territory.
    Description / Table of Contents: Übersetzung des Abstracts: Basierend auf der wissenschaftlichen Verallgemeinerung neuer Daten aus geologischen und geophysikalischen Studien sowie Tiefbohrungen beleuchtet die Sammlung die Fragen der Tektonik, der Entwicklungsgeschichte und des Öl- und Gaspotenzials einer Reihe großer Senken unterschiedlicher Art in West- und Ostsibirien und gibt auch ihre vergleichenden Eigenschaften an. Darüber hinaus bieten mehrere Artikel eine detaillierte Beschreibung der strukturell-tektonischen Merkmale und des Öl- und Gaspotenzials einiger der charakteristischsten Senken dieser Gebiete, um einige allgemeine Muster ihrer geologischen Struktur und der Lage von Öl und Gas zu identifizieren Felder auf ihrem Territorium.
    Type of Medium: Monograph available for loan
    Pages: 163 Seiten , Illustrationen , 1 Beilage
    Language: Russian
    Note: In kyrillischer Schrift
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  • 5
    Journal available for loan
    Journal available for loan
    Tübingen : Mohr Siebeck ; 1.1884 - 48.1931; N.F. 1.1932/33 - 10.1943/44(1945),3; 11.1948/49(1949) -
    Call number: ZS 22.95039
    Type of Medium: Journal available for loan
    Pages: Online-Ressource
    ISSN: 1614-0974 , 0015-2218 , 0015-2218
    Language: German , English
    Note: N.F. entfällt ab 57.2000. - Volltext auch als Teil einer Datenbank verfügbar , Ersch. ab 2000 in engl. Sprache mit dt. Hauptsacht.
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  • 6
    Monograph available for loan
    Monograph available for loan
    Stuttgart : Enke
    Associated volumes
    Call number: MR 22.94923
    In: Abriss der Geologie
    Type of Medium: Monograph available for loan
    Pages: 296 S. : Ill., graph. Darst.
    Edition: 7., verb. Aufl.
    Location: Upper compact magazine
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  • 7
    Call number: 10.1144/GSL.SP.1967.002.01.01 (e-book)
    In: Special publications / the Geological Society, London, Volume 2
    Type of Medium: 12
    Pages: 1 Online-Ressource (XI, 827 Seiten)
    Series Statement: Special publications / the Geological Society, London 2
    Language: English
    Note: Table of Contents Introduction Geological Society, London, Special Publications, 2, 1-11, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.01 The symposium meeting Geological Society, London, Special Publications, 2, 13-14, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.02 Part I: Symposium Papers Introduction to Part I Geological Society, London, Special Publications, 2, 15-16, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.03 Life in Pre-Cambrian and early Cambrian times John Watson Cowie Geological Society, London, Special Publications, 2, 17-35, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.04 The significance of certain trace-fossil ranges Roland Goldring Geological Society, London, Special Publications, 2, 37-39, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.05 Fluctuations in the evolution of Palaeozoic intertebrates Michael Robert House Geological Society, London, Special Publications, 2, 41-54, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.06 The origins of some Silurian enteletacean brachiopods Victor Gordon Walmsley Geological Society, London, Special Publications, 2, 55-56, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.07 Permo-Triassic extinction Frank Harold Trevor Rhodes Geological Society, London, Special Publications, 2, 57-76, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.08 Changes in terrestrial vertebrate faunas during the Mesozoic C. B. Cox Geological Society, London, Special Publications, 2, 77-89, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.09 Some Cretaceous-Tertiary marine faunal changes John Michael Hancock Geological Society, London, Special Publications, 2, 91-104, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.10 Major features of the evolution of echinoids Graeme Maxwell Philip Geological Society, London, Special Publications, 2, 105-106, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.11 Plant-insect relationships in Palaeozoic and later time Norman Francis Hughes and John Smart Geological Society, London, Special Publications, 2, 107-117, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.12 Biochemical evolution and the fossil record Lambert Beverly Halstead Tarlo Geological Society, London, Special Publications, 2, 119-132, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.13 Fossil birds and their adaptive radiation James Fisher Geological Society, London, Special Publications, 2, 133-154, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.14 General Discussion Geological Society, London, Special Publications, 2, 155-156, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.15 Part II: Documentation of the Fossil Record Introduction to Part II Geological Society, London, Special Publications, 2, 158-159, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.16 Plantae Plantae N. F. H. Geological Society, London, Special Publications, 2, 162, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.17 Chapter 1 Thallophyta—1 H. P. Banks, K. I. M. Chesters, N. F. Hughes, G. A. L. Johnson, H. M. Johnson and L. R. Moore Geological Society, London, Special Publications, 2, 163-180, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.18 Chapter 2 Thallophyta—2 M. Black, C. Downie, R. Ross and W. A. S. Sarjeant Geological Society, London, Special Publications, 2, 181-209, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.19 Chapter 3 Bryophyta and Charophyta* L. J. Grambast and W. S. Lacey Geological Society, London, Special Publications, 2, 211-217, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.20 Chapter 4 Pteridophyta—1 H. P. Banks, W. G. Chaloner and W. S. Lacey Geological Society, London, Special Publications, 2, 219-231, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.21 Chapter 5 Pteridophyta—2 H. P. Banks, M. G. Collett, F. R. Gnauck and N. F. Hughes Geological Society, London, Special Publications, 2, 233-245, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.22 Chapter 6 Gymnospermophyta K.L. Alvin, P. D. W. Barnard, T.M. Harris, N. F. Hughes, R. H. Wagner and A. Wesley Geological Society, London, Special Publications, 2, 247-268, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.23 Chapter 7 Angiospermae K. I. M. Chesters, F. R. Gnauck and N. F. Hughes Geological Society, London, Special Publications, 2, 269-288, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.24 Invertebrata Invertebrata M. J. S. R. Geological Society, London, Special Publications, 2, 290, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.25 Chapter 8 Protozoa F. T. Banner, W. J. Clarke, J. L. Cutbill, F. E. Eames, A. J. Lloyd, W. R. Riedel and A. H. Smout Geological Society, London, Special Publications, 2, 291-332, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.26 Chapter 9 Porifera and Archaeocyatha R. M. Finks and D. Hill Geological Society, London, Special Publications, 2, 333-345, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.27 Chapter 10 Coelenterata G. A. L. Johnson, I. D. Sutton, F. M. Taylor and G. Thomas Geological Society, London, Special Publications, 2, 347-378, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.28 Chapter 11 Bryozoa G. P. Larwood, A. W. Medd, D. E. Owen and R. Tavener-Smith Geological Society, London, Special Publications, 2, 379-395, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.29 Chapter 12 Brachiopoda D. V. Ager, P. Copper, G. M. Dunlop, G. F. Elliott, F. A. Middlemiss, A. J. Rowell, A. Williams and A. D. Wright Geological Society, London, Special Publications, 2, 397-421, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.30 Chapter 13 Mollusca: Amphineura, Monoplacophora and Gastropoda D. Curry and N. J. Morris Geological Society, London, Special Publications, 2, 423-430, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.31 Chapter 14 Mollusca: Cephalopoda (Nautiloidea) C.H. Holland Geological Society, London, Special Publications, 2, 431-443, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.32 Chapter 15 Mollusca: Cephalopoda (Ammonoidea) D. T. Donovan, F. Hodson, M. K. Howarth, M. R. House, E. T. Tozer and C. W. Wright Geological Society, London, Special Publications, 2, 445-460, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.33 Chapter 16 Mollusca: Cephalopoda (Coleoidea) D. T. Donovan and J. M. Hancock Geological Society, London, Special Publications, 2, 461-467, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.34 Chapter 17 Mollusca: Scaphopoda and Bivalvia N. J. Morris Geological Society, London, Special Publications, 2, 469-477, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.35 Chapter 18 Arthropoda: Protarthropoda and Trilobitomorpha J. W. Cowie, W. T. Dean, R. Goldring, W. D. I. Rolfe, A. W. A. Rushton, J. T. Temple and R. P. Tripp Geological Society, London, Special Publications, 2, 479-497, 1 January 1967, https://doi.org/10.1144/GSL.SP.1967.002.01.36
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  • 8
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-120
    In: Research report / Cold Regions Research and Engineering Laboratory, 120
    Description / Table of Contents: Abstract: The report is divided into four parts: Parts I and II cover investigations of the reliability of shear stress measurements in soils subjected to vibratory loads for biaxial and triaxial systems, respectively. Part I is a summary only (see USA CRREL Technical Report 90 for detailed treatment). Part III is a study of three-dimensional "principal" stress patterns produced in soil subjected to vibratory loads. Part IV is a theoretical analysis of some aspects of soil wave propagation in stratified soil. From the measurements of five shear stresses and one normal stress, the stress distribution of a triaxial system can be determined. In noncohesive soils triaxial stress fields due to vibratory loads can be determined by recording six independent stress components. Sinusoidal force excitation and impact excitation yield time-distance graphs which can be used to determine reflection and refraction techniques in stratified soils.
    Type of Medium: Series available for loan
    Pages: v, 52 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 120
    Language: English
    Note: CONTENTS Preface Summary Part I. Two-dimensional shear stress measurements Part II. Three-dimensional shear stress measurements Introduction Measurements Experimental results Evaluation Compatibility checks Comparison between shear stresses under static and dynamic loads Conclusions Part III. Three-dimensional normal stress measurements Introduction Experimental setup Results Analysis Conclusions Part IV. Soil wave propagation in stratified soil Introduttion Distance-time graphs Results Sinusoidal force excitation Refraction Impact force excitation Selected bibliography Appendix A. Equations for computing stress components in Part II Appendix B. Equations for computer program in Part III
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  • 9
    Call number: MOP 41085 / Mitte
    Type of Medium: Monograph available for loan
    Pages: XIII, 144 Seiten , Illustrationen
    Language: English
    Location: MOP - must be ordered
    Branch Library: GFZ Library
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  • 10
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-202-77
    In: Research report / Cold Regions Research and Engineering Laboratory, 77
    Description / Table of Contents: Abstract: A deep rotary core drilling project in 1957 at Site 2 on the Greenland ice sheet (76°59'N, 56°04'W provided ice core to a depth of 411 m. The vertical variation in bulk density, macroscopic structure, oxygen isotope ratios, ionic constituents, and extraterrestrial dust (black spherules) were analyzed using both field and laboratory techniques . These data permit the direct estimate of annual accumulation layers in the core. Continuous stratigraphic measurements and observations were made over the upper 110 m of the profile and detailed physical and chemical analyses were made on continuous lo 3 to 3.9-m core increments at 100, 200, 300 and 411-m depths. The average total ionic concentration in the ice sheet ranges between 0.65 and 1.35 mg/liter. The annual global mass deposit of black spherules as calculated from these studies varies from 2.10 x 10^5 metric tons in 700 year old ice to 6.57 x 10^5 metric tons in 12 year old firn. The oxygen isotope ratio variation provides the best means of estimating accumulation at depth. Results of the investigations indicate rates of net snow accumulation of 42.3, 34.2, 37.4, 41.1 and 41.6 g/cm^2 -yr at the surface, A.D. c. 1773, c. 1513, c. 1233 and c. 934 respectively. Accumulation data and other physical and chemical evidence allow climatological inferences to be made over the 10-century profile. The ice core record shows that snow accumulation and temperature in A. D. 934 were similar to today, followed by a gradual decrease in accumulation to a minimum around the late 18th century and an increase in both accumulation and temperature from A. D. 1773 to 1957 and following.
    Type of Medium: Series available for loan
    Pages: vi, 130 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 77
    Language: English
    Note: CONTENTS Preface Summary 1. lntroduction General background Previous work The Greenland Ice sheet Present work Ice core studies ll. Field procedures General background Subsurface snow laboratory Core reference datum Core handling and processing Ill. Macroscopic stratigraphy General background Polar stratigraphy General observations and results Discussion of results and conclusions above 100 m IV. Detailed stratigraphic studies General background Macroscopic stratigraphy at 100 m Results of analysis and discussion Summary and conclusions V. Oxygen isotope studies General background Previous work Deep ice core 0-isotope stratigraphy Results of analyses Summary and conclusions Vl. Chemical composition studies General background Previous work Factors influencing the chemistry of glaciers Deep core stratigraphy using chemical variations Results of analyses and discussion Summary and interpretation of the 300 m results Geochemistry of the ice sheet Results of analyses and discussion Summary and conclusions Vll. Cosmic dust studies General background Previous work Origin of extraterrestrial dust Deep ice core and near surface studies Results of analyses Discussion of results Summary and conclusions VIII. Climatological implications General background Recent history of the inland ice Past history from the deep core Summary and conclusions- IX. Summary and conclusions Discussion Post Site l deep drilling programs Selected bibliography Appendix A. Sorge's law Appendix B. Thinning of layers Appendix C. Statistical terms Appendix D. Average density determinations for meter increments from the surface to 411.21 meters , Site 2, Greenland
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